EAGER: Are the Dry Valleys Getting Wetter? A Preliminary Assessment of Wetness Across the McMurdo Dry Valleys Landscape

智力价值：直到最近，干燥山谷中的湿润土壤通常只在溪流和湖泊附近发现。自从2002年温暖的南夏以来，有多少湿润的地方？在远离海岸线的相对平坦的谷底位置，以及谷壁上向下流动的指状物被观测到。湿润这些土壤的水的来源以及年复一年发生的空间和时间模式都不清楚。它们的意义可能是巨大的，因为增加的土壤水分可能会改变表层土壤的热力学、水文学和侵蚀速度，并促进以前稳定的物质的运输。土壤活跃层的这些变化可以显著改变干旱河谷内的永久冻土和地面冰的稳定性。PI试图调查这些变化，以解决两个相互矛盾的假设：这些湿点的水源？地面冰正在融化，而这些水的来源是积雪融化。PIS将使用Quickbird和Wordview卫星的高频遥感数据记录这些湿润地区的时空动态，以记录2010-11和2011-12南半球夏季湿点的发生、尺寸和增长。他们将通过确定湿点是否在每个季节的相同位置重复出现来检验他们的假设，并使用存档图像比较现在和过去的分布。他们还将确定空间积雪模式和时间消融模式是否与湿点形成一致。更广泛的影响：一名研究生将接受该项目的培训。研究结果将在科学会议上报告，并发表在同行评议的期刊上。他们还将为水文学促进单元课程开发一个关于水文学遥感应用的教学模块，以及一个创新的原型项目，该项目旨在通过使用社交媒体和移动计算应用程序，利用公众参与绘制干旱山谷中的湿点和雪地地图。

Intellectual Merit: Until recently, wetted soils in the Dry Valleys were generally only found adjacent to streams and lakes. Since the warm austral summer of 2002, numerous ?wet spots? have been observed far from shorelines on relatively flat valley floor locations and as downslope fingers of flow on valley walls. The source of the water to wet these soils is unclear, as is the spatial and temporal pattern of occurrence from year to year. Their significance is potentially great as enhanced soil moisture may change the thermodynamics, hydrology, and erosion rate of surface soils, and facilitate transport of materials that had previously been stable. These changes to the soil active layer could significantly modify permafrost and ground ice stability within the Dry Valleys. The PIs seek to investigate these changes to address two competing hypotheses: that the source of water to these ?wet spots? is ground ice melt and that the source of this water is snowmelt. The PIs will document the spatiotemporal dynamics of these wet areas using high frequency remote sensing data from Quickbird and Wordview satellites to document the occurrence, dimensions, and growth of wet spots during the 2010-­11 and 2011-­12 austral summers. They will test their hypotheses by determining whether wet spots recur in the same locations in each season, and they will compare present to past distribution using archived imagery. They will also determine whether spatial snow accumulation patterns and temporal ablation patterns are coincident with wet spot formation. Broader impacts: One graduate student will be trained on this project. Findings will be reported at scientific meetings and published in peer reviewed journals. They will also develop a teaching module on remote sensing applications to hydrology for the Modular Curriculum for Hydrologic Advancement and an innovative prototype project designed to leverage public participation in mapping wet spots and snow patches across the Dry Valleys through the use of social media and mobile computing applications.